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本文依据红土台地、高盆地和111个Q_3晚期海相泥炭层、23个Q_3晚期滨海相地层、9个Q_4海滩岩等资料,初步探讨了莆仙平原—兴化湾的发育演变及其地震的关系。
Based on the information such as laterite terraces, high basins and 111 Q 3 late marine peat layers, 23 late Q 3 marine facies strata and 9 Q_4 beach rocks, the paper discusses the development and evolution of the Puxian Plain - Xinghua Bay and its earthquakes Relationship.